High-temperature, low-H2O Silicic Magmas of the Yellowstone Hotspot: an Experimental Study of Rhyolite from the Bruneau–Jarbidge Eruptive Center, Central Snake River Plain, USA

High-temperature, low-H2O Silicic Magmas of the Yellowstone Hotspot: an Experimental Study of Rhyolite from the Bruneau–Jarbidge Eruptive Center, Central Snake River Plain, USA

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Veröffentlicht in:Journal of petrology 2012-09, Vol.53 (9), p.1837-1866
Hauptverfasser: Almeev, Renat R., Bolte, Torsten, Nash, Barbara P., Holtz, François, Erdmann, Martin, Cathey, Henrietta E.
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container_issue 9
container_start_page 1837
container_title Journal of petrology
container_volume 53
creator Almeev, Renat R.
Bolte, Torsten
Nash, Barbara P.
Holtz, François
Erdmann, Martin
Cathey, Henrietta E.
description
doi_str_mv 10.1093/petrology/egs035
format Article
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source Oxford University Press Journals All Titles (1996-Current); EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection; Free Full-Text Journals in Chemistry
title High-temperature, low-H2O Silicic Magmas of the Yellowstone Hotspot: an Experimental Study of Rhyolite from the Bruneau–Jarbidge Eruptive Center, Central Snake River Plain, USA
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